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Twenty-Third Symposium on Naval Hydrodynamics (2001)
Naval Studies Board (NSB)

Page
540
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Page
540
Front Matter (R1-R19)
Modern Seakeeping Computations for Ships (1-45)
Forces, Moment and Wave Pattern for Naval Combatant in Regular Head Waves (46-65)
New Green-Function Method to Predict Wave-Induced Ship Motions and Loads (66-81)
Validation of Time-Domain Prediction of Motion, Sea Load, and Hull Pressure of a Frigate in Regular Waves (82-97)
Ship Motions and Loads in Large Waves (98-111)
Prediction of Vertical-Plane Wave Loading and Ship Responses in High Seas (112-125)
Basic Studies of Water on Deck (126-142)
Second Order Waves Generated by Ship Motions (143-156)
Prediction of Nonlinear Motions of High-Speed Vessels in Oblique Waves (157-170)
Optimizing Turbulence Generation for Controlling Pressure Recovery in Submarine Launchways (171-180)
Hull Design by CAD/CFD Simulation (181-190)
Steady-State Hydrodynamics of High-Speed Vessels with a Transom Stern (191-205)
Practical CFD Applications to Design of a Wave Cancellation Multihull Ship (206-222)
Simulation of Ship Maneuvers Using Recursive Neural Networks (223-242)
Flow- and Wave-Field Optimization of Surface Combatants Using CFD-Based Optimization Methods (243-261)
Marine Propulsor Noise Investigations in the Hydroacoustic Water Tunnel 'G.T.H.' (262-283)
Propulsor Design Using Clebsch Formulation (284-300)
Unsteady Flow Quantities on Two-Dimensional Foils: Experimental and Numerical Results (301-313)
Hydrofoil Turbulent Boundary Layer Separation at High Reynolds Numbers (314-329)
Pressure Fluctuation on Finite Flat Plate Above Wing in Sinusoidal Gust (330-341)
Control of the Turbulent Wake of an Appended Streamlined Body (342-354)
Investigation of Global and Local Flow Details by a Fully Three-Dimensional Seakeeping Method (355-367)
Prediction of Wave Pressure and Loads on Actual Ships by the Enhanced Unified Theory (368-384)
Frequency Domain Numerical and Experimental Investigation of Forward Speed Radiation by Ships (385-401)
International Collaboration on Benchmark CFD Validation Data for Surface Combatant DTMB Model 5415 (402-422)
Validation of High Reynolds Number, Unsteady Multi-Phase CFD Modeling for Naval Applications (423-440)
Free Surface Viscous Flow Computation Around A Transom Stern Ship by Chimera Overlapping Scheme (441-456)
Anti-Roll Tank Simulations With A Volume of Fluid (VOF) Based Navier-Stokes Solver (457-473)
Validation of Tab Assisted Control Surface Computation (474-484)
Experimental and Numerical Investigation of the Flow Around the Appendices of a Whitbread 60 Sailing Yacht (485-492)
Propeller Wake Analysis by Means of PIV (493-510)
Experimental and Numerical Investigation of the Unsteady Flow Around a Propeller (511-526)
Simulation of Incompressible Viscous Flow Around a Ducted Propeller Using a RANS Equation Solver (527-539)
On Submerged Stagnation Points and Bow Vortices Generation (540-552)
Numerical Prediction of Scale Effects in Ship Stern Flows with Eddy-Viscosity Turbulence Models (553-568)
The Experimental and Numerical Study of Flow Structure and Water Noise Caused by Roughness of a Body (569-578)
Large-Eddy Simulations of Turbulent Wake Flows (579-598)
Instability of Partial Cavitation: A Numerical/Experimental Approach (599-615)
An Unsteady Three-Dimensional Euler Solver Coupled with a Cavitating Propeller Analysis Method (616-638)
On the Flow Structure, Tip Leakage Cavitation Inception and Associated Noise (639-653)
An Experimental Investigation of Cavitation Inception and Development of Partial Sheet Cavaties on Two-Dimensional Hydrofoils (654-669)
Modeling 3D Unsteady Sheet Cavities Using a Coupled UnRANS-BEM code (670-686)
Ship Wake Detectability in the Ocean Turbulent Environment (687-703)
An Experimental and Computational Study of the Effects of Propulsion on the Free-Surface Flow Astern of Model 5415 (704-712)
Breaking Waves in the Ocean and Around Ships (713-745)
Numerical and Experimental Study of the Wave Breaking Generated by a Submerged Hydrofoil (746-761)
The Numerical Simulation of Ship Waves Using Cartesian Grid Methods (762-779)
Radiation Loads on a Cylinder Oscillating in Pycnocline (780-791)
Wave Resistance Computations - A Comparison of Different Approaches (792-804)
Computations of Nonlinear Turbulent Free Surface Flows Using the Parallel Uncle Code (805-819)
Submarine Maneuverability Assessment Using Computational Fluid Dynamic Tools (820-832)
Simulation of UUV Recovery Hydrodynamics (833-847)
Reynolds-Averaged Modeling of High-Froude-Number Free Surface Jets (848-862)
On Roll Hydrodynamics of Cylinders Fitted with Bilge Keels (863-880)
Combining Accuracy and Effciency with Robustness in Ship Stern Flow Computation (882-896)
An Unstructured Multielement Solution Algorithm for Complex Geometry Hydrodynamic Simulations (897-909)
Ship Stern Flow Calculations on Overlapping Composite Grids (910-926)
Study on the Prediction of Flow Characteristics Around a Ship Hull (927-940)
Analysis of Turbulence Free-Surface Flow Around Hulls in Shallow Water Channel by a Level-Set Method (941-956)
A Design Tool for High Speed Ferries Washes (957-967)
Flow Around Ships Sailing in Shallow Water - Experimental and Numerical Results (968-982)
Ship Stability Study in the Coastal Region: New Coastal Wave Model Coupled with a Dynamic Stability Model (983-992)
Waves and Forces Caused by Oscillation of a Floating Body Determined Through a Unified Nonlinear Shallow-Water Theory (993-1005)

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On Submerged Stagnation Points and Bow Vortices Generation L. R~eja (Indian institute of Technology, Khara Dur, India) AflSTltACT Th mechmi m of the genemti m of bow vertices in two dbm nsi ms, m hbomtory scale, is expkmed on th basis of th :xistence of c subm rged tagrution pomt below fhe fiee smtcce Th t~eam which originctes from fhe submerged tagrution poi t m fhe fie smtcce di ecti m reverses md neut~ali es th mom nt m of mcommg flow ~esultmg m c flee su face separction pomt Th miticl location of fhe submerged stagmtion pomt md subsequently fhe flee smiace separction pomt is cclcubted for fhe case of c s misubmerged horizontal cimukr cylmd r, md fhe ktter is compmed wifh th experime tal results The cgrement is ~ecsonably good Th generction of bow vo tices is ddscussed as c balance betweff~ mertial md gravitational effects Th loss of pressure et fhe b w md th consequent d cg due to b w vertices phffmm mr is calcuhted md is fommd to cgre w 11 with th value fommd by exper ime t A medho do logy for th de sign of efhcient b w contour shap in two dimff~siom whe~e fhe subm rged stagnati m point is used es c conhol hmdle, is p~esented The fheory is clso mplied to nm~egmbr shcpes Ike vetical step md bulbous b w Th results are compared with fhose obtamed by flow computati m md found to be m ~easonably close cg~e ment Firully, c conject re is cd cnced to expkm th genemti m of bow vo tices m the dimff~siom, i e fhe neckk e vo t :x arommd c ship's load waterlme, on the same basis INTRODUCTION Th vo ticcl moti m observed checd of c particlly submerged object tow d m c hyd odynamic tmk is k ow as bow vertices The bow vo tices ~egion is separcted fi m fhe mcm potential flow by c shc,m boundary termed es fhe flee su face separcti m poi t FSSP), when fhe flow is two dimem iorul Th hyd odynamic flmmes The understmdmg of fhis ph n menon is of di~ect comeq ence to bow wave b~eaki g, which is re pomible for c substmticl c mpone t of c ship's resirtfmce Bcbc 1969) The ph n menon d picts itself in the form of white water et th bow contmumg cll arommd the ship's load waterlme, md is also called es neckk e vo t :x Seve~al mfhors hcve isuclised bow vortices checd of two dimensiorul es w 11 es thee dimff~sionai shap s, eg E k t md Sharma(1970), Smuki (197~9, Honji, (1976, Shchshalkm (1951), b'~yo md Tckekumc (1951), b'~yo, Takekuma, Eggers, Sharmc (1952) md Mori (1954) But, h re w shell be primarily concemed wifh the experiments of b'~yo, Tckekumc, Eggers md Sharmc (I 952) on c hori ontal semi subm rged cimukr cylinder c mducted et Imtit t f r Schiflb m, Hcmburg it may be relev mt to m nti m f tt fhe mfhor hcs iewed the videotape of fhese e perim nts b fhese e perim nts, c cacukr cylmder was tow d m c hori ontal semisubmerged condbti m (two dimff~sionai flow) md fhe bow vo tices w ~e visualised usmg c watercolour dye Th FSSP was mecsmed for diffe~e t vulues of d cit Froude mmmber F~) Th primaryobjectiveofthispcp ristoe pkm fhese ~esults qualitatively md q mtitatively But befcre fnat, w shell p~esent c brief review of th cttempts mcd so far in this du ectioa Dcgen md Tulm (1972) solved th g~avity fl w pc t c blmmt body by usi g two pert rbati m e pensions A mcll Froud mmmber solution was obtcined fcr the flow mmder the mmbrokff~ fiee smtcce upto second crder, while c high Froud m mber solution was obtamed based upon fhe mod I of c jet detachmg fi m th bow md not retmomg to fhe fl w The heakmg of fhe wave was cssigned to Tcylor mstability d e to fhe tepff~mg of fhe sheamlmes A

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critical F~ was obtcined to characterise th omet of wa~ b~eaki g Th cssocicted d cg due to b~eaki g of waves was also calcubted md was found to be twice fhe value estimated by Bcbc (1969) experime tally Mori (1984) assigned fhe white water gff~erction phenomffmn to she fl w imtability md subsequent b~eakmg of fhe bow flow, md tudied th same themeticclly md experime tally m g~ecter detail The fiee smtcce cmvatme was concluded to be one of th somces of sh ar fl w benecth th fie surtcce Stability am~lysis, vcrticity shetchi g fheory, md fiee su face boundary kyer fheob w ~e mvolved to expkm fhe exp rimental results, eg velocities, Rey old shesses md b w wave heights Pctel, mdweber md Tmg (1984) cttempted to expkm fhe b w vo tices genemtion on th basis of fhe :xistence of c fie smtcce bommdary kyer, which is c kyer of concenbated vorticity occunmg due to fhe curvat re of fhe fie smiace m fhe fl w of c ~ecl fluid Th cuthors sp cuhted f tt fhe fiee surtcce would move slower f m th kyer benecth it md fhis velocity defect would lecd to c FSSP checd of th body md subseq e tly fhe bow vo tices Fu ther, by assmmmg fnat et th fiee smiace th smtcce tensi m is baLmced by ncrmal viscous shess fcrce, m exp~essi m for FSSF locati m was obtcined by d6'ect mtegmti m of fhe boundary c mdition using th contim ity quctioa The locati m of fhe FSSF was obtcined m terms of fhe slop of fhe fie smtcce Th ~esults so obtamed were cpplied to c cimukr cylmd r md compmed wifh th exp rim ntal values of b'~yo et cl (1982) The fheoretical vulues show d m inc~ecsi g t~end, ie fhe FSSF will move cway fi m th body with mcrese in d cft Froud m mber while exp rim ntal results pomted to fhe ~everse H wever, fhe e perim nts of Grosenbmgh md Yemmg(1985,1989) ~eported good cg~eem nt wifh fheir separcti m criterion The idec of c fiee smtcce boundary kyer lecd6 g to c FSSF was fmfher examined by Rahqc (1995) The fie surtcce boundary Icyer velocity md vo ticity proflles w ~e computed et various stati ms up t~eam it was observed thct fhe fie smtcce moved slower f m th flow beneadh it but fhis velocity defect was not large ffmugh to ~esult m c FSSF ahecd of th body Yeu g md Ammthakrishnfm (1992), in their computaticrur tudy of fhe probl m (to be dscussed hter), also conclud d fnat th fiee smtcce vo ticity is not mtense ffmugh to lecd to bow vo tices The bommdary kyer vcrticity proflles computed by Rahejc (1995 poi ted towards mstability of th boundary Icyer flow owl g to fheu nommonot mic rutme VmdeeBroeck & Tuck (1977), Vmdn Broeck, Schwart md Tuck (1978) contmued mvestigati ms mto the cnalytical solution of th bow fl w problem by usmg c series e pension m Froud m mber, but conclud d f tt it was not possible to obtcin c co tmuous bow wave proflle becmse of nm mmiqueness of th soluti m However, th bow shape was reshicted to bows wifh c ve ticcl or mclmed flct faced They pecubted thct fhe possible fomm of soluti m for fhese shmes is thct of m ovetmomg jet Tuck md VmdeeBroeck (1984) show d fnat c co tmuous splashless bow flow was possible fcr some diffe~e t bow shap s such as bulbous bow it was cssum d cll though that th tag,nction poi t lies et fhe mtersection of th body md fhe fiee su face The difhculty in fmdmg c closed for solution gave m impetus to computatiorul st dies Miyata et al (1985) mplied c version of th M C method to ccpt ~e nmlinear wave breaking et th b w The nonlmear waves b~eaki g et th bow due to tepness w re temmed as fiee smtcce shock wave FSSW) The exact n mlinear fiee smtcce condti m was used et fhe flee bommdary md fhe no slip c mditi m on fhe body A computational st dy, which gives mme msight mto fhe bow flow, is fnat of Grosenb mgh md Yemmg (I 989) These mfhors have used c boundary mteg~al medhod to compute fhe two dimff~sional flee su face flow pest c semi i fmite body m th time domcia The fie smtcce c mputation is done accordmg to th m fhod give by Lo guet Higgms md Cokelet (1976 The criticcl Froud mmmber F~ fcr fhe omet of wa~ b~eaki g is found for bow shcpes vertical step, faued body md bulbous b w It is fommd th re fnat c bulb m the b w shape delcys the omet of wave b~eakmg In fhis tudy, th flee surtcce fl w is developed fiom the tecdy tate double body fl w th s avoidmg th impulsive tart of the body which may result m unco trolled bow wa~ elevatioa This is also supported by th fmdmg of Dcgen & Tulm (1972) where th low st order asymptotic expmsi m of th fie smtcce flow pest s mi mflmte body is found to be c double body flow wifh fhe fie smtcce repk cd by c rigid pkte Besid s, it seems quite logical to c msider c stecdy state double body flowas fhe miticl c mditi m; fhe suddenly r mo i g fhe upper hclf of fhe flow cllows th flow to develop to c fiee smtcce fl w The mfhors also discuss th occm~ence of submerged tagrution pomt(SSF) on th body, which behaves differently for fhe b~eaki g regime md non b~eaki g regime of fhe flow For th fcrm r case, the SSF r mcms bel w fhe flee smtcce while th bow wa~ overt ms, but fcr th ktter, fhe SSF is miticlly bel w fhe fiee su face md rises to fhe flee smtcce as

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fhe bow elevation ~educes md settles et th tagrution height of O SF~2 We shell discuss fhese ~esults ktter in moth r section of th work Yeung md A mbnaloish m (1992) mvestigated fhe fl w of c ~ecl fluid past c two dimff~sional bow, one of the cim bemg to examine fhe possibility of b w vo tices observed et kborctob sccle The mfhors concluded thct th occmrence of b w vertices in th kborctcry scale is due to th p~esence of surfactmts which accmmubte near th body md pro id rigid bommdary I kc behcviom to fhe fiee surtcce ledmg to boundary ky r separcti m md subsequently vertices The N. 5 equctiom coupled wifh th su factmt conce tmti m eqrcti m w ~e computed by c varictiorul flactiorul tep method md usmg fhe no slip condition et th fie surtcce, fhe occm~ence of vo tices was show Th mfhors clso mvestigated fhe case of fie slip md th exact nonlmear flee smtcce boundary condition md arrived et fhe conclusion thct vorticity genemted due to fiee sutcce cmvatme is not i tff~se enough to lecd to separction As c rece t development, Dong, b'~t &Humg (1997) hcve usedPIV to visualise th bow flow md mesured th flow velocities near fhe bow wa~, upshem md dow t~eam The laser sh et is visualised m differe t orientati ms checd of fhe bow md et different stations dow sheam of fhe bow Smmmarismg th above ~e i w, one may menti m fnat fhe ideas of Tcylor in tability, fie surtcce bommdary kyer md su fact mt conce tmti m have ben emmmed but th mechmi m of bow vertices generction md fhe occunence of fhe FSSP are still not w 11 understood md to th be t of om k owledge th results of fhe e perime ts by b'~yo et al (1952) have not yet ben e pkmed A two dimff~sional tudy is c msidered clmo t c necessary tep m fhe developme t of c th °b for fhe f e dimff~sional case, es it provides c valuable gam m msight et fhe expff~se of rehtively simple computatioa The~efme, it is desuable to conce tmte on fmdmg c theob fcr e phim g th e perim ntal ~esults of b'~yo et cl (1952) befme discussmg th f ee dimemiorul generction of white water, neckdace vo t:x or b w wave b~eaki g in m oce m goi g ship b fhe p~esent work, w propose c th °b to expkm fhe bow vo bees genemtmn m th kborctcry scale m two dimff~sional fl w on fhe basis of th occunence of c subm rged stagnation pomt (SSP) This is cnalyticclly found for fhe flow pest c semisubmerged hori ontal cacular cylinder Subsequently, th cppro imate vulues of th PSSP for different d cit based Proud mmmbers me cclcubted md compared wifh fhe e perim ntal values of b'~yo et cl (1952) Pu th r, th d cg due to loss of pressme et th bow is cclcubted md c mpared wifh th value estimated by Bcbc (1969) e perim ntally Besid s c cacukr cylmd r, th fhecry is clso cpplied to c vertical tep md c bulbous b w shme Th design of m effcient bow contom m two dimff~siom is discussed Pinally, c conject ~e is cd cnced fcr e pkmmg fhe f ee dimemiorul bow vertices generctioa The subseqre t sections of fhis pmer develop th idec md fhe relevmt expressiom m c tep by tep manner ff~dmg with conclusi ms md f t ~e scope of work SSP THEORY AND BOW VORTICES GENERATION The mech ml m of bow vertices genemti m md fhe occmrff~ce of th fie su face separcti m poi t c m be exphined und r fhe fiamework of th proposed SSP th °b as follows A tagrution pomt m fhe two dimff~sional flow pc t c f lly submerged object is clways fhe mtersection of th di id6 g t~eamlme md the body The sheam divides itself mto two parts et this pomt Th pressme on bodh fhe sides of fhe tag,nction poi t d meases The pomt is c maximum of fhe p~essure dish ibution b fhe case of fhe flow pest c partially subm rged object, c tagnation pomt may :xist below th fie su face md may be rightly called c submerged stagnati m pomt (SSP) es show m Pig I It may be conject ~ed fnat m case m SSP does :xi t it should similarly be th mtersection of fhe di id6 g sheamlme md fhe body Accordmgly, the sheam should d6 id itself mto two parts et fhis poi t md ff th fl w is two dimff~sional, one part will flow below fhe object md fhe of her should move upward m fhe d6'ection of fhe fie surtcce This ktter part of th sheam, wi g to th obvious limitation in mo i g upward due to g~avity, ~everses md neabalises fhe velocity of fhe incomi g fl w ~esultmg m m PSSP where fhe two velocities c me m baknce Th reversmg flow tmps c regi m offhefluid(Fig l)extff~dmghori o tallyfrombody to th PSSP md verticclly fi m the SSP to fhe fie surtcce P, duly bommded by th d6 id6 g sheamline md the fie su face such thct fhe fluid is mo i g clo g fhe boundary of fhis regi m, i e fiom PSSP to SSP clo g th d6 id6 g sheamline, from SSP to P clo g fhe body md fmclly toward PSSP clong the fie smiace The cucubtion of fhe fluid clong th boundary of fhis regi m sets th entue mass of th h mped fluid mto cyclic motion givmg rise to fhe flrst vertex wifh positive i e mti clockwise vorticity et fhe cenhe which may be due to only i terrul sh ar The vo tex grows in si e md fcr stability reasom, c see md vertex starts from fhe body sid with rotati m m fhe opposite duecti m Thus fhe fluid k eps m

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yl -: ~t- ssP ~' Fig I Scbm rged shgnstioc poict (ssP) sad the sssocisted bow vordces gece~tioc ic the dow psst s hortrochl semisubme ged circcEr cylinder entermg m fhis regi m fi m fhe body side due to th upward mo ing tt am, md fhe vo tices me contimtously produced fi om body sid The boundary FSSP fhus keeps on shiftmg slowly tmmmd upsheam as th regi m is filled Fu th r, mwi g to this fluid fllli g, th bow wa~ height contmuously mcreases md upsets fhe inerticl g c itatiorui baknce which t suits m e pelli g fhe flrst vo t :x out of fhe regi m to jom th main flmw with fhe FSSF mm i g backward md th bow wa~ height comi g dmvrt simmltaneously, md fhe process of fllli g th regi m t starts The oscillation m bow wave height md th cort pondi g back md fo th moveme t of fhe FSSF have ben obsetved e perime tclly by Grosenb mgh md Yeu g (1955,1989) md clso by fhe present mfhor m m op n~u cu thti g water charmel (unpublished) Th s, fhe fluid keps on enteri g fhis t gion from th upward mm mg sheam md th vmtices are contmu tsly prodt cd from body sid md expelled fi m fhe of her sid to jom th mcm tt tm This, in c mttshell explaim th mech ml m of bmw vmtices gff~erction md fhe occunff~ce of th FSSF The sit ation described above cone p mds to fhe case whert fhe fiee t face is not brokert in case fhe ft e t face heks, fhe upward mm mg sheam fi m fhe SSF fomms c bmw jet, which enhaim air md dismteg ates to fmm bubbles, reversmg i to th mcm flow cgain t sultmg m th FSSF Vmdet Broeck md Tuck (1977) had specubted c simibr scenario as one of th possibilities while cttemptmg to flnd m am~lyticcl soluti m for verticcl or inclit d flat faced bmw shcpes FtESULTS AND DISCUSSION SSP -Evisteue cud Locetiou To confum the e i tff~ce of m SSF md tbs qtt ntly fmd its position should t quit, m genemi, solvi g fhe glavity flmw problem, which of c trse, is very difft uit But it is possible to k ow cbout fhe SSF md evert flnd fhe mitial location of th SSF by amrlysi g the mitial c mdition of fhe probi m Com ider fhe two dimertsimuri flow pc t c horizontci semi tbm rged cit ukr cylinder it is cssum d ft~t fhe fiee t face flow is obtamed by mitistly he i g potential double body flow md removmg th upper flmw suddertly at m imt mt (t = 0+) which may be ttkert as the omet of gm ity flow (Grosenbmgh md Yemmg 19S9) Hff~ce the pres tre md fhe velocity fleid pt vaiimg imticily, i e et t = 0, me th s k mvrt md it is possible to se wh fher m SSF e i ts md cal thte fhe iocati m of th SSF which wiii th n be fhe pomt wh re fhe total pt s tre wiii have its maximum on the body it may be me tioned ft dt th fie smtcce flow at t = 0+ is d tbie body flow solution of fhe Lmk e quation wifh fhe pt s tt t pkt d by total pt s tt, i e mciudi g gravity term Referring to fhe axis sy t m es show t m Fig I, for fhe tt am flowmg m fhe positive x dit ction, the mitici pres tre di tribution, i e at tim t = 0+, at my poi t (x, y) in fhe flmw wlli be given by totci pt s tt ~s P=Pat +OSp(U~ U2) psy (1)

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wh re U is fhe velocity of the flow, md U~ is th velocity far upshem md P~h, is ctmo pheric p~essme Fcr th pomts on fhe cylmd r, w k ow fi m th ~esults of pote ticl double body flow fnat U=2U~ smO' (2) wh re O' is the polar coordincte of fhe pomt mesured fi m fhe positive x axis Fmfher, y=RsmO wh re R is fhe ~adms of fhe cylinder (3) Fcr th present problem, fhe domain of mterest fcr O'wouldbe :rsO's 2 Th refcre, w d flne c new varicble O as 0=0' :r so f tt fhe domcm of mterest of O cone pondmgly bee mes O s O s :r /2 which is more convenient fcr arurlysis b hod cmg(2) & (3) mto (I),w obtain p=pa,,+OSpU2(1 4sin20)+pgRsmO (5 N w n m dbm nsicrurlismg th dist mces with R md fhe p~essmes with O SpU~ md retami g th same notatiom for noedimff~sionalised variables, w get p = Pab~ + (I 4 sin O )+ F ~ d wh re Fd is d aft based Froude mmmber defmed as F U~ Eqrction (6) gives fhe prevailmg p~essme dishibution on th submerged part of fhe cylmder contour at th mset of fhe g c ity flow The maximc md mmimc of fhis p~essme d6 tributi m cm be (~ obtained by fhe cor~ntiorul method ie putti g P =0 dO which leds to cosO ( 3sinO + ~ )= 0 The points of optimum pressure will be given by 0 = 2 md sin0 = ~ (g) It is import mt to note fnat in fhe second case, fcr O to be memmgf 1, one mmst have Fd >0 5 (9) However, th re is no re triction m Fd bei g large even upto oo Frocedmg f th r to ch ck the maximc md mmima, w fmd fhe second derivative, (4) d~p zo 2smO ~ = 3+16sm dO Fd (1 o) Evaluati g (10) fcr fhe vulues of O obtamed m (3), w get P = g _ for 0 =— dO~ Fd 2 (11) d P= g+_4 forO=sin ~— (12) d O 2 Fd 4 Fd Keepmg fhe resh icti m given by (9) m mmd, w flnd fnat (11) gives c positive defmite md (12) gives c negative defmite value for Fd ~ 0 5 b of her words, fhe pressure has c maximmm at 0 = sin (1/ 4Fd ) md cmmimum ctfhe bottom mo t point 0 =:r/2 m fhe domain OsO s:r/2 it may be pomted out fnat for Fd = 0 5, (11) md (12) bodh give zero, co fumi g (9) in fact for Fd = 0 5, only one maximmm occurs et O=:r/2 mth domcm OsOS:r,whilefor Fd more th m O 5, fhere is c cone pondi g maximum et :r O Hence w conclude th~t for Fd '0 5, th re is maximum m fhe pressme d6 tributi m et 0 = sm ~ (1/ 4Fd ). md ob iously this poi t is the

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tbm rged stagnation point Th pressme decreases on bodh sid s of it, so the velocity mu t be zero Table I placed in fhe section on Bmw Dmg) gives fhe locati m of th SSP md fhe cort pondmg vallt oft ndimertsionalpt s tt cceffcientdefm dinth conventimurlwayas Cp = P Pat )/0SpU~ different vulues of F~ it may be observed ft~t for F~ =05,th SSPisat O=:r/2,th Imvestpointofth cylmd r As Pt inct cses, th SSP moves upward towards th fiee smtcce md flnally for Fd =°°, 0 = 0, i e SSP coincides with fhe t tgnation poi t of d tble body flow, th n p~,,, is duly t placed by p~ fhe defmition of C~ This t tit will be discussed f th r in c latter section m inerticl gm itatimur balance PresmreProDde cud Ftow witb SSP — Ow C .] O _ o ~ ilss~ ~ \ ~ss~ 0 / N\, ~to- / ~1 ~ \ Fig 2 Prosscro distriLctioc beforo (t = 0 ) sad st tho ocsot of gravih tow (t = 0~) for tho dow psst s hortrochl somisubm rgod circclsr cylindor Tho mdisl distanco m sscrod from tho body givos tho v~lue of Cp A t piccl pt s tre di tributi m befot md et fhe omet of g c ity flow, for F~ = 0 5 md I O is show t m Pig 2 The pressut coeffcient at fhe pomts on th co t tr is givert by fhe mdial distance fi m fhe pomt to fhe cmve it may be obsetved ft dt m th case of double body flow (t=O:, th pt ssut umfommly decreses from A to D, but et fhe mset of gm ity flmw i e t=0, the pt s tre increses fi m A to SSP md th n d et ases to D The SSP oc trs et O =1445°forF~=10 Thept s tt dct csesonbodh sides of fhe SSP Conseq ently, at fhe onset of gm ity flow, fhe fluid particles, above th SSP will mm upwards md below fhe SSP will move dm~rds Th upward mm mg tt am will t verse owmg to fhe limitati m d e to glavity, t tltmg m th PSSP md bow vo tices provided th t face is not brokert, as expkmedin mearlier secti m Celenhtdou of FSSP The PSSP is creted when th flow fi m SSP to P Pig 1) t verses md its velocity comes m balance wifh th incomi g flow velocity clo g th fie trface The velocity of th t verse flow at th poi t A (fhe stagnation pomt of the d tble body flow) et th mset of glavity flow m be cclculated by mplymg Bert ulli's eqtwti m et fhe SSP md et th poi t A The fommer bemg c stagnati m pomt of th gm ity flmw, fhe velocity is zero th re md fhet fot w get P)i = P)~ +V (13) where V is th velocity of th upward flow et A Th pt ssut P)DSI! md p)~ c m be obt tined by tb titutmg 0 = 0D~, md 0 = 0 t sp ctively m eq ction (6) Accord6 gly, w obtam V2= 4F~ (1 4) So far w hcve ben obtammg fhe t tits just by cnalysmg th imticl condition, es it was pe t tim g to fhe mset of glavity flow m immediately fhereafer; but th next tep i e bahmci g fhe t verse flow cgam t fhe mcommg flow clo g fhe fie trface, is c t suit belongmg to fhe flnal tecdy state, which c m be achieved mly cider severcl smeller tim steps fi m th time t = 0+ onward b fhese steps, th fiee trtcce conditi m is to be cpplied on fhe fiee smtcce, fhe mcommg md reverse flow is to be cclculated clo g fhe ft e su face which itself is m urJmow t Of fhe problem The t n Imearity of fhe ft e smiace c mditi m tdd c futher complicatiot However, sit th cim of fhe p mer is to present fhe fhemy md e pkm fhe m chmism of bow vortices genemtim, md t t to go into det tiled c mputation, w shell tb to obttm some cppro imate re tits so as to get m msight i to fhe phertom nm Accordmgly if ;~ is fhe slope of th fiee smiace w m w ite th balancmg process es COS ;~ = Uz (1 s)

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wh re U~ is th x velocity component of th double body flow slo g fhe x axis Substitutmg U~=l (I/x2) fmth caseof fhecacularcylmdr,(l5 leldsto ~ vssr = 1~ As poi ted out, it is not possible to Imow th cmt et value of ;~, so w shall assmme het ftmt ;~ = 0, which msy be valid for t latively small values of Froud mmber Cmseqtt ntlyw obtsin | 2Fd d (17 Fm obtsmmg rel vallt s of x fi m (17 w mmst have Fd >— (= 0 71) V: (I g) Hence fhe vulidity of (17 starts from 071 mteld of O 5 which is fhe natmal re triction for fhe csse of s cit ular cylmd r qn 9) it msy be noted ftmt th validity rightly improves ff (16) is used m place of (17) b this case, w obt tin in placed of (I g) Fd > 47 (1 9) Smce cos;~ < I mywh t on th fie t face, th rhs will slways be less thm 1/4i, md fm ;~ = 60, fhe t sult Fd >1/2 is obtsmed But, as mentioned earlier, th fiee su face slop md th velocities of th incomi g md reverse flmws me to be cal tlated togedher, so myhmg less f m fhe full flow c mputation will not do md my sppro imste value of fie smisce slop will lesd to m enoneous t sult Thet fot, w accept fhe t d ced validity of fhe fmmuh (17) for fhe FSSF for th pt sent C omp ens o u wit b E spenmeut sd Results Th mtmerical values of xp~ ss obtsmed fi m (17) are d Iy conve ted to d (=x I)Fig 1, md plotted slo g with fhe experimental vulues in Fig 3 A trve has beert passed f oughth e perimental poi ts of b'myo et al md is show t tgsm t fhe trve obt tined fi m present fheory The observatiom c m be smmmed up ss follows ~ ~~~= ;4 52 OG OS Ot 10 Fig 3 Free smtace sepsmtim poict (FSSF) ic the t ow psst s semisubme ged horimchl cirmEr cylinde~Experimect md Theo y (i) The FSSF moves closer to fhe body m conflmmstion with th exp rimental re tlts qttalitatively (ii) The exp rim ntal vallt s fm Ft < 0 5 se m to be flt t stmg md do not behave m s t gular fashion ss fhe values for Ft > 05 This msy be related to th fact ftmt s w 11 defmed SSF does not e i t for Ft < 0 5 ss it doesforFd>O5(cf Bqn 9) (iii) The th ot tical values for Ft = 0 72 to 12 cm be ssid to be ressotmbly close to th e perim ntal trve keepi g fhe cmde basis of fheu derivati m m mmd luer~dld-Gre titedomtl Effect It is intere tmg to obsetve fhe ch mge m the location of fhe SSF md the FSSF wifh fhe met sse m Ft As Ft is mcressed, th SSF mm s closer to the fie trface md fhe FSSF moves closer to fhe body, Fig 4 Th region, which is obt tined by jommg fhe SSF, th FSSF md F (obt tined by taki g bmw wa~

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height ss 0 5 F42 ) which is s t gi m of tmpp d fluid contsmmg bow vortices, sh irJcs wifh fhe mct ase of Ft Fig 4 Vsrisdon in the bow vortices region with F4 The region is torm d by ~oining SSF iocstions t the corre Fonding FSSF iocstions sad hidDg the nse ot ft e su face = 0 5 F4 tt the cylmder This c m be expl tit d ss foil ws: Th origm of fhis happ d vortex t gion is fhe effect of glavity Th Froude m mber represents th r ttio of inertis fot e to glavity fot e Vhen Ft is it essed, th gm ity effect t Ittively red ces md fhet by th t gion shmks b fhe limiti g csse of Ft = oo th t gion fmally mishes with fhe SSF commg st 0 = 0 md th FSSF also coming st p = 0, i e m th body Th fl w thert behaves like double body flow This is quite logical, ss m fhe sbset of glavity, fhe flow should behave like double body fl w Th bow wa~ height 0 SF42 becomes mfmite but fhis is dtt to th fact ft~t Ft is th d tft based Froude m mber md for Ft ~ °°, w mmst have d aft bec mmg zero, which mdic ttes ft gt fhet is no gravity actmg my mot md so no bow wave BowDrag Smce fhere is s t verse flow betwen th poi t A md th SSF Fig 1), fhet will be s 1oss of pt ssut md sssocitted b w dag, which cm be obt tined by mtegmti g th x component of th force dtt to pt ssme fiom A to fhe SSF Accordmgly, th b w d sg D is given by ssr D= | P Pat )n~ds wh re n~, is th x duection cosine md d is fhe mc cl me t Het n~=cosO mdth vallt of P Pat mbe tb tituted fi m (5 By doing so w obt tin CD I = | (I 45iD 0+— 2 pU~B O [d _, sin0)cosR dO (201 which on perfommmg fhe t quit d mtegmti m md usi g (8) for 0ssr, gives d [ d ] (21) The sbove formuh c m slso be wwitten in terms of fhe SSF mdth Froud mmber,ie C I [ I + g ~ 0 ] The sbove fomm is, m s way, c mparsble to th one obt tined by Dsgert md Tulin (I 972, B m 72) One c m slso expt ss CD as s f nction of fhe SSF only md obt tin CD = sin°sss [I + 3 sm 05sS ] (22) (23) Table I gives fhe values of CD for diffet t Ft values md slso 6he cort pondmg locstion of th SSF The obset ttions me as foil ws: e 90.00 44.00 JO.67 23.tt.3 18 00 . 1447 1193 1000 6.37 4.97 o~333 F. 0.5 0.6 0.7 0.8 0.9 10 1.1 1.2 1.5 1.7 20 ~ _ Tshle I The iocstion ot subm rged st gnsdon point (9sw) with the couesponding vslue ot S st the onset ot grwth t ow sad the nOn dim nsionsl vslue ot bow d~g (CD) tor di ferent v~ues ot F4 tor the csse ot semi subm rged hortront~ circulsr cytinder C 5 tl0 2.93 204 t 33 1.25 1.17 112 1.05 1.03 102 100 CD 1 3 667 1 1.588 o 864 1 0 552 1 0.387 0.292 1 0.234 1 0.115 1 0 088 1 0~ o.oo 1 I The mtmerical values in Table I sh w 6~t CD dect sses when th d tft Fr tde mmmber mct ases, which w tld m m 6~t higher th d tft Froude m mber, 6he lower 6he b w d tg At 6he fust mstmt this does not sppesl to th c mm m und rstfmdmg of d sg vs peed t latiomhip But, it c m be i terpt ted simply m

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temms of mertial g~avibtiork~l effect as discussed earlier As F~ inc~eases, th me tie effects ~ektively rise over g ~ lty effects md bow d ag, bei g ~ comeqrence of gravity effect, ~educes This is f th r clear fi m fhe location of fhe SSP which moves closer to fhe fiee smface wifh mmease of F~ md fhus reduces fhe r mge SSP to A Fig 4) which is ~e pom ible for inc~easi g th kmetic energy of th surroundmg water by gff~eratmg ~everse flow md subseqre tly bow vortices/bow jeVwhite water 2 Th re is no ekborate experlme tal data a~ilable to c mpare fhe values m Table I However, Baba (1969) hes suggested ~ two dbm nsiom~l ~ep~esenbtion of heakmg wa~s for his e perlme ts on ~ t mker, as ff it was mmiform md normal to th bow, md has estimated its eqflvale t le gfh as roughly helf fhe beam Dagff~ & Tulin 1972) Th d ag coefficie t, per umt lengfh, cone pondmg to ~ two dbm nsiom~l fl w across th b~eaki g wave for F~= 1 7 is given as CD (= Dl O SU~ T)= 0 08, wh re D is th d ag md T fhe d ~'d Baba 1969 § 7 3) b teresti gly, w fmd fnat our value of CD for F~ = 1 7 comes out as 0 088 Table 1), which is very close to fhe estimate of Baba This closeness of CD vulue obtained by fhe p~esent fheory with th one estimated fiom e perim nbl ~esults f th r pro id s support to fhe SSF th °b e pkmmg fhe mechmism of b w votices gff~eration it may be ~elevmt to m ntion fnat Dagen & Tulin (1972) obtained fhis value of CD = 0 17 (about two times) for ~ ve tical step by sol i g fhe gravity fl w usi g fhe method of two pert rbation exp msiom 3 Bow d ag dep nd upon fhe location of fhe SSF, fhe low r fhe SSF th mme is th bow d ag Th location of fhe SSF on th oth r h md is, d6'ectly ~ekted to th p~essme ddshibutim of double body fl w on fhe bow, which m t rn dep nd upon its shme The~efme, th double body p~essme d6 tributi m on th b w md fhe locati m of fhe SSF pro id fhe key to fhe desig of b w co tour for minlmmm b w d ag Bow Cout~mr Deslgu -two dlmeusloual ease A bow contour for th two dlmemiorul case m be designed now for mmlmum b w d ag as foll ws Th total pressure at my pomt of th bow is fhe sum of double body pressure md fhe gm lty p~essme, i e Cp(~ly =cp(d6) +cre The c mdition for fmdmg SSF is given by aCp(b~l) O ay which gives aCp(d&) = dy (25) acpe dy b gene~al Cp(d &) is maxlmmm at fhe double body tagnation pomt DBSF) md decreses toward th bottom as fhe fluid accelerates The g ~ lty pressure, on th of her hmd is zero at fhe mmdist rbed fie surface (i e at DBSF) md mcreses toward th bottom Owl g to fhe opposite sigm of fhe rate of chmge of fhese two p~essmes, ~ maximum m Cp (~1) (i e fhe SSF) occms at fhe poi t whe~e th two rates of chmge me eqral in magmt de, makl g fhemteofchmgeof CP(~I) tobezero (26) The rate of ch mge of double body p~essure is indep nd nt of F~ md depends pmely up m th geometb or fhe slopes of fhe bow co tour at d6ffe~ent poi ts On th of her hmd fhe mte of chmge of gm lty p~essme is 2/Fd which is comtmt dependmg upon daid based Froud mmber Th SSF location is given by fhe mtersection of fhe two sides of (26) when plotted wifh ~esp et to y Now by usi g ~ double body flow calcubtion prog amme by suibble panel medhod md coupli g it with ~ curve design progmmme usi g Bezier curve B splme wifh ~ visual interface, it should be possible to d sig b w contom which gives fhe SSF locati m as near th fi e smface as possible for ~ given value of F~ it may be desuable to tag th process wifh the selection of design d fd of th ship This will give fhe scope of m mipubtion of fhe mte of ch mge of g ~ lty p~essme additionally Thus th locati m of SSF acts as ~ conhol hmdDe for fhe desig of m efhcient bow contour md also serves as ~ measme of pe formance with regard to b w d ag Foracacularcylmdr Fig l),w cmwite(25)as CP (~U) = 1 4Y ~ Y md mplymg fhe procedme as descril~d above based on (26) fhe location of SSF is shalghbway obbmed analytically as (27)

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Fig 6 shows th location of SSP m fhe case (2g) of th ve ticcl step for differe t d cid Froud m mbers 4 F~2 l Y= Th cpplicati m of fhe above to of her shapes is shmvrt belmw SSP for Ve ttieel Step cud Bulbous bow So far w have ben usmg c t gmbr shap, ie c cu thr cylinder, for fhe cpplication of th proposed fheob it is so becmse w hcve th experime tal results fm th cu tlar cylmder But th fheory c m be cpplied to of her bmw shapes tually w 11 md whatever t suits are obt tined arulyticclly m fhe case of th cu tlar cylmder, cm be obtamed m mericclly in fhe case of t m gular two dimertsional bow shapes As m example, w pt sent here fhe application of th th °b to c ve tical tep md c bulbous bmw shcpe Th geomeby of th verticcl step md th bulbous bow hcs beert ttkert fi m Grosenbaugh md Y tog(l959) The d tble body flmw is cclculated usmg c low ord r panel method Fig 5 show th cmves of C (tb) md th C (totcl) for Ft=l Fig 5 The vsnstioc of C~(db) sad C~(~t) vs Dmd forvert(cs( s step sad Bc(bocs bow Th shmpchmgesinth slop mditsduectimmfhe geometb are d Iy reflected m fhe culve of C (tb ) at fhe cmt spond6 g pomts The maximc occunmg m fhe culve of totcl pressut m be esily marked s, Wi ~ t, t t, j F(g 6 Determ(mt(oc of subm rged shgnst(oc po(cts for s vert(cs( step The vert(cs( ((ces show the s(ope of gm ih comFocect of presscre Det rmicst(oc of submerged shgnst(oc po(cts for s bc(bocs bow The Vert(m( ((ces show the s(ope of grw(h comFocect of presscre determit d by fhe procedme based on (26) md described in th earlier section i e by d cwmg th slop cmve of C (tb ) md fhe con t mt slope Imes of C fm d6fferent vallt s of Ft The i tersecti m of the two slope ttves fhert gives th cmrespond6ng SSF locatiot it c m be seen thct es Ft mcreases, fhe SSF m th ve tical tep moves closer to fhe fie smtcce, simibr to fhe case of c cit ular cylmd r For Ft = 1, fhe SSF lies c little above half th d cid, which is c mparable to th value es show t by Grosenb mgh md Y t g (I 9S9) with fhe flmw computatiot Fig 7 shows fhe sarne for fhe case of bulbous bmw shcpe Owmg to th fi tuent chmges in fhe dbt ction of slop m fhe shap, fhe maximc me not es w 11

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defned es m th case of fhe verticcl step For example, for F~ = 1, fhere are two maxlmc md two mmlm~ Accordmgly th flow pict ~e will be mme complicated f m as hcs l~en d scribed for the case of fhe cucular cylmd r m verticcl step But, smce th see md maxlmc hcs fhe higher value of C Oobr) fnat should be bken es th hue maximum md be fhe SSF m th cunent context it is fhen observed fnat th SSF for fhe bulbous bow shcpe is low r thm m th case of fhe verticcl tep for fhe same value of F~ = I This provides m exphnati m for th observation ~epmted by Grosenbmgh md Yeu g (1959) fnat th wa~ hekmg is delcyed for c bulbous b w relative to c ve tical step, smce low r is fhe SSF fhe less doml mt is th mertic effect md wa~ brekmg which is duectly Imked wlfh sped is debyed accordmgly Bow Vor~des - tb ree dlmeuslousd eese Th foami g motion or white water observed at fhe b w of c ship md cll clong th load waterline k wn es neckkce vo t x, is th thee dlmff~sional pict ~e of bow vortices if th bow vmtices me genemted in fhe two dim nsicrurl case by fhe presff~ce of m SSF l~low fhe fiee su face, it will be just right to conject ~e fnat m SSF may xist et fhe ship's b w md et th secti ms l~low th fie surtcce b of her wmd, th curve of C omr) vs d aft may have c maximum et th b w md et fhe sections Smce fhe ship has c fmite d cid, its double body flow must acqune c c mpone t of velocity m fhe depfh duection right fi m fhe forward perp ndlcukr down th hull Accordmgly, et th b w fhere is c d mecse of double body pressure fi m forward pemff~dicukr to th kel md et each secti m fi m load waterlme to th bilge, which in presence of gm lty, ~esults m c SSF bel w th fie smtcce givmg rise to c fl w fi m fhe SSF to fhe fie smtcce This upward flow may fmm c jet et the fiee smiace, enbam c lot of air md dismteg ate i to immm rable bubbles at fhe fiee su face ~eflecting mme light owing to their k ge smtcce are md form c white water or c foam lik mpe ance Coueluslous Th problem of b w vo tices genemtion et kboratmy scale is cdd essed h re with fhe mcm clm to e pkm fhe ~esults of fhe experiments on c hml ontal semisubm rgedcacular cylmd r, md fhe mechmism of bow vortices genemti m observed ahecd of fhe cylinder I it is shown fnat fhere xists c tagnation pomt bel w fhe fie suface, ie c submerged sbgnation poi t (SSF) which is resp msible for makmg c bmnch of fhe mcm t~eam flow upward towards th fiee su face md fhus produce c ~everse fl w which results m bow vmtices md c f~ee surface sepamti m pomt FSSF) 2 The SSF is c f nction of d cid based Froud mmber F~ md double body p~essme dishibutioa The SSF occms whff~ th double body pressure d meases along th d cid md c msequently, c maxlmmm mpears m th tobl p~essme below fhe fiee smtcce it is fmfher discussed fnat th location of the SSF represents c balance l~tween mertial effects md g~avity effects The SSF moves towmds fhe fie smtcce as F~ is mmeased md only fm F~ = oo (i e no g c lty, mly inertlc) SSF lies on fhe fiee smtcce comcidmg wifh fhe sbgnati m pomt of double body flow 3 The values of FSSF cclculated on th basis of fhis fheory for flow past c horl o tal semi submerged cacuk cylmder e pkm the e perim nbl ~esults of b'myo et al (1952) qualibtively md q mtitatively to c recsonable e tent 4 The bow d cg is obbmed es c fm tion of d cft based Froude mmber The value of the bow d cg for F~ = 1 7 for fhe case of c cimuk cylmder, cgres very w ii wlfh th value e tlmated by Bcbc (1969) by e perim nts on c tsrD~r md fmdmg c two dim nsiorul equivalent of fhe same 5 It hcs beff~ conject red thct fhe bow vo tices m fhe f e dlmemiorul case, ie th neckkce vmtex m c ship, me also produced by fhe sarne c msideration Owmg to c fmite d cid, fhere is c c mpone t of velocity m fhe depth duection m double body flow of th ship which lecds to c decrecse of double body flow p~essme fi m forward pemendicuk to keel et fhe bow md fi om waterlme to bilge at sections This results m c SSF et fhe b w md et fhe sections below fhe f~ee smtcce Th flow from fhis SSF towards fhe fiee su face results in c jet et the fiee su face, which ent~ams air md fmms bubbles makmg white water m c foam like cppeamnce

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Scope of tbe future work I C mputstiorul st dbes are ~equned to be undertakff~ to verify fhe ~esults of this th °b Fu t, fhe fl w past c horizontcl se iisubmerged cucukr cylmd r should be computed md th SSP location, ~eversal of flow, th FSSP location md fhe bow d cg be calculated md checked wifh fhe results obtcined by th fhecry 2 The experime ts m c horizontcl semisubmerged cacukr cylmder should be ~epeted md fhe bow vortices should be visualised md st dbed m fhe light of the p~esent fheory The SSP location should be found md fhe m~t ~e of reverse fl w should be st dbed Th PSSP locati m should be found md compared with th fhecry The oscillatiom m fhe PSSP locati m md cone pondi g bow wa~ height should be st dbed Also, fhe b w d cg should be found exp rim ntclly md checked withth fheory 3 Th steps (1) md (2) should be c mducted fcr odher bow ge mehies with different slop dishibution, e g verticcl step, conventicrur ships bow md bulbous b w et 4 Th conjectme mcde fcr bow vo tices gff~erction in c f ee dimemiorul case is to be verifled by usmg c the dbm nsicrurl arulyticcl body generated by c k own combination of singmbrities The flow past c sphe~e or Rmkine ovul do not serve fhe pu pose es th se me axisymm hic Th c mbination should be such as to result m c hue f ee dimff~sional fl w This will ~equne fhe dishibution to be asymm hic Alternatively, fhe double body p~essmes may be computed m c Wigley hull usi g c higher ord r pmel method so fnat th poi ts et fhe bow c m be tsken as nodes es w 11 as collocation pomts md fhen th p~essme dishibution et fhe b w md at th section should be obbmed Subs quently, fhe SSP et fhe bow md et fhe sections should be calcubted to conflmm fhe genemti m of bow vertices in th f ee dimff~sional case We have worked wifh fhe values of C for double body flow for c series 60 h 11 obtcined fiom "SB P PLOW" but fhese w ~e et th panel cc troids which w ~e cway from fhe pomts at fhe b w contour Owmg to fhe high tmgential velocity m th neighbourhood of bow, fhe C was far bel w th expected value of umty et DBSP We used c four/five deg~ee smiace flttmg but th exhapokti m was not sati factory Refereues Bcbc, E "A New C mpone t of Viscous Resistmce of Ships" Journal of the Socieh of Ncval A chitects of Jcp m, Vol. 125,1969, pp 23 32 E kc t, E md Sharmc, 5 D "Bugw I te fur Lmgsame, Vollige Schiffe" Jahrbuch der Schiffl mtechmisch n Gesselschcf Vol. 64, 1970, pp 129 171 Smuki, K, "On fhe Drag of Two Dim nsicrurl B o db es 5 m isubmerged m c P' ee Su face P low" Jomrurl of Society of Ncval A chitects of Japcn, Vol. 137, 1975,pp 22 35 Honji, H "Observation of c Vertex m fro t of c Hclf submerged Cucular Cylmd r" Journal of th Phvsiccl Societv of Japcn, Vol. 40, 1976, pp 5 ShahshaLfm, A "A St dy of Pre Smtcce Plow Near c Ship Bow", MS thesis, b tit te of Hyd mlic Research The Universih of lowc, lowc Cih, lowa, 198l Kcyo, Y. md Tamekmmc, K "On fhe P'ee Smtcce Sh ar Pl w Rekted B w Wa~ B'eaki g of Pull Ship Models" Journal of th Societv of Ncval A chitects of Jm m, Vol. 149, 19S 1, pp 11 Kcyo, Y. Takekmmar, K, Eggers, K md Sharmc, 5 D "Observation of Pre Su face Shear Plow md its Rektion to B w Wa~ B'eaki g on Pull Pcrms" Bericht No 420, b titut f r Schiff m. Umversih of Hcmburg,Hambmg,Germmv, 1952 Mori, K H "Neckk e Vo tex md B w Wa~ A ound Blunt Bodies" P oceed6 gs, 15th ONR 5 mosimm on Ncval Hvd odvnamics, Hcmburg, Gemm my Sept 2 7, 1954 Dcgen, G md Tulm, M P. "Two dimff~sional P'ee surtcce Gravih Plow Pc t Blunt Bodies", Jomrurl of PluidMech Vol. 51,1972,pp 529 543 Patel, V C, Lmdweber, L md Tmg, C J. "Pre Smiace Boundary Lcyer md th Origm of Bow Vo tices" Proceedmos. 2 d b ternaticrur 5 mposimm m Viscous Resi tance, SSPA, Goteborg, Sw den, 19S5 Grosenbmgh, M A md Yemmg, R. W. "Plow Shuct re Near c Ship Bow" Renort No NAOE S5 1, ONR Co hact No N00014 54 K 0 26, Univ: of Cclifcrnic, USA, Oct. 1955

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Grosenbmgh M A md Yemmg, R. W. "Flow Shp t ~e Ne fhe Bpw of Two Dim nsippcl Bodbes" Jomrul of Ship Rese~ch, Vol. 33, 19S9, pp 269 283 Rahqc,L R. "Fre Su face Bommdary Lcyer Approach to St dy Bpw Vo tices G perction Ahecd of c S misubmerged Horizontal Cu phr Cylinder", Joup~l of Ship Rese h, Vol. 39, No 4, Dee 1995, pp 284 296 Yemmg, R. W. md A mfPckrishp m, F "Vorticcl Motipm wifh md wifhout c Smtcce Fiercmg Body" Froced6nigs, 19th 5 mposimm pm Naval Hvd odvnamics, Seoul, Kp e, 1992 V md p Broeck, J. M md Tuck E 0 "Computatiom of Ne Bow md Stem Flows Usmg Series E pensions m the Froude Number", F oc 2 d I ti Cord: On Num rical Shin Hvd odvnamics, Berkeley, Califp ma, 1977, pp 377 357 V md p Broeck, J. M ,Schwart, L W. md Tuck, E O "Divergent Low Froude Number Series E pensions of Npmlip ar Fre Surtcce Flow Froblems", Froc R. Sp Lpmd Vol. A361, 1975, pp 207 224: Tuck, E 0 md V mdep Broeck, J. M "Splashless Bow Flows m Two Dim psiom", 15th S mposimm on Na~l Hvd odvnamics, 1954, pp 293 3 0 1 Miyata, H. Nishimmc, 5 "Fmite Diffe~ep Simulation of Nop Imear Ship Waves", Joup~l of Fluid Mech mics, Vol. 157,1955, pp 327 357 Grosenbmgh M A md Yeu g, R W. "Nonimear F'ee Smtcce Flow et c Two Dim psioncl Bow" Joup~l of Fluid Mech mics, Vol. 209,1959, pp 57 Longp t Higgms, M S. md Cokelet, E D "Th Defp mation of Step Smtcce Waves on Wcter", I A m mericcl medhod of computatiop Froc R. Sp Lpmdop A350,1976,pp 1 26 Dong, R. R. Kctz, J. md Hu mg, T. T. "On th Shp t re of Bow Waves on c Ship Model", Joup~l of FluidMechmics,Vol 346, 1997,pp 77 115

Representative terms from entire chapter:

fhe ssf